METEOROLOGY
... Inversion in the stratosphere is due to heating of stratosphere from the absorption of UV rays by O3; absence of O3 ---- air would become colder with height • Mesosphere: Extremely thin air, low pressure and density; average temp. ~-90°C; • Thermosphere: Hot layer above Mesosphere; very few atoms an ...
... Inversion in the stratosphere is due to heating of stratosphere from the absorption of UV rays by O3; absence of O3 ---- air would become colder with height • Mesosphere: Extremely thin air, low pressure and density; average temp. ~-90°C; • Thermosphere: Hot layer above Mesosphere; very few atoms an ...
Powerpoint
... • Inversion in the stratosphere is due to heating of stratosphere from the absorption of UV rays by O3; absence of O3 ---- air would become colder with height • Mesosphere: Extremely thin air, low pressure and density; average temp. ~-90°C; • Thermosphere: Hot layer above Mesosphere; very few atoms ...
... • Inversion in the stratosphere is due to heating of stratosphere from the absorption of UV rays by O3; absence of O3 ---- air would become colder with height • Mesosphere: Extremely thin air, low pressure and density; average temp. ~-90°C; • Thermosphere: Hot layer above Mesosphere; very few atoms ...
the earth`s spheres
... fundamental recycling processes are photosynthesis, respiration, and the fixing of nitrogen by certain bacteria. Disruption of basic ecological activities in the biosphere can result from pollution. 5. The Atmosphere (air sphere) is the envelope of air that surrounds the whole Earth. The mixture of ...
... fundamental recycling processes are photosynthesis, respiration, and the fixing of nitrogen by certain bacteria. Disruption of basic ecological activities in the biosphere can result from pollution. 5. The Atmosphere (air sphere) is the envelope of air that surrounds the whole Earth. The mixture of ...
Overview of the Earth`s Atmosphere
... wind chill, frostbite and hypothermia heat exhaustion and heat stroke cold spells, dry spells and heat waves severe thunderstorms and flash floods • The mathematical formula for determining the wind chill temperature has recently been revised due to new ...
... wind chill, frostbite and hypothermia heat exhaustion and heat stroke cold spells, dry spells and heat waves severe thunderstorms and flash floods • The mathematical formula for determining the wind chill temperature has recently been revised due to new ...
The Earth and Its Atmosphere
... greenhouse effect = warming that results when solar radiation is trapped by the atmosphere; caused by atmospheric gases that allow sunshine to pass through but absorb heat that is radiated back from the warmed surface of the earth. Water is the only substance that can be found naturally in the atmos ...
... greenhouse effect = warming that results when solar radiation is trapped by the atmosphere; caused by atmospheric gases that allow sunshine to pass through but absorb heat that is radiated back from the warmed surface of the earth. Water is the only substance that can be found naturally in the atmos ...
Climate Change
... • Climate – the average atmospheric conditions over longer periods of time. Sometimes referred to as the weather of the world. ...
... • Climate – the average atmospheric conditions over longer periods of time. Sometimes referred to as the weather of the world. ...
The Dynamic Earth
... the continuous movement of water on the Earth Evaporation – water heated by the sun rises into the atmosphere Condensation – water in the atmosphere cools and forms water droplets on dust particles Precipitation – larger water droplets fall from clouds ...
... the continuous movement of water on the Earth Evaporation – water heated by the sun rises into the atmosphere Condensation – water in the atmosphere cools and forms water droplets on dust particles Precipitation – larger water droplets fall from clouds ...
Characteristics of the Atmosphere
... from the air as part of their life processes. Living things, burning, and weathering would quickly use up most atmospheric oxygen if it were not for various processes that add oxygen to air. Land and ocean plants produce large quantities of oxygen in daylight. ...
... from the air as part of their life processes. Living things, burning, and weathering would quickly use up most atmospheric oxygen if it were not for various processes that add oxygen to air. Land and ocean plants produce large quantities of oxygen in daylight. ...
4-1 Role of Climate
... Greenhouse Effect A. CO2, methane, water vapor, and other gases trap heat energy and maintain Earth’s temperature range. B. A natural insulating blanket of gases that trap sun light from escaping into space. C. Solar energy penetrates the atmosphere and is converted to heat energy and then some ra ...
... Greenhouse Effect A. CO2, methane, water vapor, and other gases trap heat energy and maintain Earth’s temperature range. B. A natural insulating blanket of gases that trap sun light from escaping into space. C. Solar energy penetrates the atmosphere and is converted to heat energy and then some ra ...
File
... and cools down more slowly than land. Knowing this, which of the following statements is most likely true? A. On a sunny day, the air over a piece of land will be cooler than the air over a bordering lake. B. On a sunny day, the air over a lake will be cooler than the air over the bordering land. C. ...
... and cools down more slowly than land. Knowing this, which of the following statements is most likely true? A. On a sunny day, the air over a piece of land will be cooler than the air over a bordering lake. B. On a sunny day, the air over a lake will be cooler than the air over the bordering land. C. ...
ppt - Earth and Space Sciences at the University of Washington
... sun’s radiation into atomic oxygen and eventually formed ozone . • Ozone absorbed most of harmful ultraviolet radiation to make Earth suitable for life. ...
... sun’s radiation into atomic oxygen and eventually formed ozone . • Ozone absorbed most of harmful ultraviolet radiation to make Earth suitable for life. ...
The Dynamic Earth Ch. 3 Sect. 1 Objectives Describe the
... Ex: water vapor, carbon dioxide, methane, nitrous oxide 3.Trapped heat radiated back to Earth’s surface, warming the air. Without this Earth would be too cold to live on However, too many greenhouse gases can trap too much heat. Sect. 3 Objectives Name the three major processes in the water cycle. D ...
... Ex: water vapor, carbon dioxide, methane, nitrous oxide 3.Trapped heat radiated back to Earth’s surface, warming the air. Without this Earth would be too cold to live on However, too many greenhouse gases can trap too much heat. Sect. 3 Objectives Name the three major processes in the water cycle. D ...
Climate Change – Chapter 7
... This movement of air affects global ____________________ and ____________________ patterns. The _______________________ is the collective mass of water found on, under, and over the surface of Earth in the form of liquid water, ice, and water vapour. Water that is carried into space is not part of t ...
... This movement of air affects global ____________________ and ____________________ patterns. The _______________________ is the collective mass of water found on, under, and over the surface of Earth in the form of liquid water, ice, and water vapour. Water that is carried into space is not part of t ...
OUR PLANET
... • The atmosphere is made up of several layers. Most of the air we breathe is in the bottom layer called the troposphere. This extends for 12 miles (20 kms) above the Earth´s surface. The farthest layer from Earth is the exosphere, which has very little gas.Also it has the stratosphere (ozone layer) ...
... • The atmosphere is made up of several layers. Most of the air we breathe is in the bottom layer called the troposphere. This extends for 12 miles (20 kms) above the Earth´s surface. The farthest layer from Earth is the exosphere, which has very little gas.Also it has the stratosphere (ozone layer) ...
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... It is the theory that Earth’s surface cracked into plates millions of years ago and these plates have been moving and shifting ever since. ...
... It is the theory that Earth’s surface cracked into plates millions of years ago and these plates have been moving and shifting ever since. ...
The wind we experience on Earth occurs primarily in the “Planetary
... Layer” in the “Troposphere” and is bounded vertically at high altitudes by the “tropopause”. ...
... Layer” in the “Troposphere” and is bounded vertically at high altitudes by the “tropopause”. ...
EnvSci Chapter 3 Review Answers
... What is the temperature of the inner core? _4000oC -5000oC_ (make sure you give a unit!) What causes the inner core to be solid? _intense pressure_ In which geologic zone is 1/3 of the Earth’s mass found? _The Core (both Inner and Outer Core)_ Where does most geologic activity happen? _Tectonic plat ...
... What is the temperature of the inner core? _4000oC -5000oC_ (make sure you give a unit!) What causes the inner core to be solid? _intense pressure_ In which geologic zone is 1/3 of the Earth’s mass found? _The Core (both Inner and Outer Core)_ Where does most geologic activity happen? _Tectonic plat ...
The Atmosphere - Cobb Learning
... increases, air pressure decreases also changes as altitude increases due to the way solar energy is absorbed as it moves through the atmosphere • High % of gases that absorb solar energy= warmer • Less gases that absorb solar energy= cooler ...
... increases, air pressure decreases also changes as altitude increases due to the way solar energy is absorbed as it moves through the atmosphere • High % of gases that absorb solar energy= warmer • Less gases that absorb solar energy= cooler ...
Atmosphere of Earth
The atmosphere of Earth is the layer of gases surrounding the planet Earth that is retained by Earth's gravity. The atmosphere protects life on Earth by absorbing ultraviolet solar radiation, warming the surface through heat retention (greenhouse effect), and reducing temperature extremes between day and night (the diurnal temperature variation).The common name air is given to the atmospheric gases used in breathing and photosynthesis. By volume, dry air contains 78.09% nitrogen, 20.95% oxygen, 0.93% argon, 0.039% carbon dioxide, and small amounts of other gases. Air also contains a variable amount of water vapor, on average around 1% at sea level, and 0.4% over the entire atmosphere. Air content and atmospheric pressure vary at different layers, and air suitable for the survival of terrestrial plants and terrestrial animals is found only in Earth's troposphere and artificial atmospheres.The atmosphere has a mass of about 5.15×1018 kg, three quarters of which is within about 11 km (6.8 mi; 36,000 ft) of the surface. The atmosphere becomes thinner and thinner with increasing altitude, with no definite boundary between the atmosphere and outer space. The Kármán line, at 100 km (62 mi), or 1.57% of Earth's radius, is often used as the border between the atmosphere and outer space. Atmospheric effects become noticeable during atmospheric reentry of spacecraft at an altitude of around 120 km (75 mi). Several layers can be distinguished in the atmosphere, based on characteristics such as temperature and composition.The study of Earth's atmosphere and its processes is called atmospheric science (aerology). Early pioneers in the field include Léon Teisserenc de Bort and Richard Assmann.